... River, Ontario, and Pinawa, Manitoba, and at a research area, also on granitic terrane, near White Lake, Ontario, where work was done early in the program to test geophysical exploration and borehole-logging equipment.The ability to predict subsurface geological and hydrogeological conditions at future...

..., the Connecticut River Valley has rich historical archives from Hitchcock’s era, including several town historical societies, the Pocumtuck Valley Historical Society, and the archives of regional colleges, especially Amherst College. As illustrated by this book and by McMaster’s website, many of these resources...

... unpublished reports ( Hunter, 1980 ; Leckie, 1981b ; Bullock, 1980 ; Walker, 1982 ). REFERENCES CITED Bullock , A. , 1980 , Sedimentation of the Wapiabi-Belly River transition (Upper Cretaceous) at Lundbreck Falls, Alberta : B.Sc. thesis, McMaster Univ . Hunter , D. F. , 1980...

.... Many of the foraminiferal species of the McIntosh formation are identical with, and many others are similar to, those illustrated and discussed by Cushman and McMasters (1936) from McMasters’ Llajas formation of California. Laiming (1940) has designated the Llajas fauna of Cushman and McMasters...

... (McMaster, Lachance & Ashraf 1970). At the present day many active rivers reach the coast in Sierra Leone but little modern deposition takes place on the middle and outer shelf, since the sediment load is trapped in estuaries and Late Precambrian and Phanerozoic geology of Sierra Leone 615 LAYER 1 t LAYER 2...

...Robert L. McMaster; Eric Christofferson; Asaf Ashraf Abstract Magnetic and seismic-reflection surveys have revealed the presence of faults and basic intrusive rocks, two open-ended shelf basins, a drowned delta, unconformities, a distorted sediment zone, nonuniform prograding, and slumps and slides...

..., 1968 ; Ewing et al. , 1963 ; Garrison, 1970 ; Hoskins. 1967 ; Knott and Hoskins, 1968 ; McMaster et al. , 1970 ; Mc-Master and LaChance, 1968 ; Meisburger and Duane, 1969 ; Moore and Curray, 1963 ). Such a complex origin of the shelf’s edge is confirmed by the present detailed study...

... incised off larger rivers inshore but has little relief toward the shelf-break. This difference results from the steep gradient of the inner shelf and the gentle gradient of the valley's long profile. Incision was caused by high fluvial discharge during sea level fall. Decline of discharge and sediment...

... Copyright © 1975, The Canadian Society of Petroleum Geologists 1975 BULLETIN OF CANADIAN PETROLEUM GEOLOG Y VOL . 23, NO . 2 (JUNE 1975), P . 340-34 8 BIBLIOGRAPHY OF THESE S DEPARTMENT OF GEOLOG Y MCMASTER UNIVERSITY Ph.D. Theses Anderson, P. A. M., 1968, Phase relations of the hydroxyl...

... Division of Pure Chemistry, National Research Council, Ottawa. 3 Hamilton College, McMaster University. The writers are indebted to the Imperial Oil Company and the National Research Council of Canada for financial assistance. Also they thank Parke A. Dickey of The Carter Oil Company, Tulsa...

... Succession and variation of Monotis and the associated fauna in the Norian Pine River Bridge section, British Columbia. (Triassic, Pelecypoda) Journal of Paleontology 36 745 792 Westermann G. E. G. 1963...

... deltas, including the Rio Grande and Mississippi deltas. The deltas were recognized by geomorphic pattern, high-angle clinoform seismic reflections, and association with buried river systems. Isopach patterns show that the deltas range in size up to 5,000 km 2 (1,900 mi 2 ) and reach thicknesses of over...

... and Dusenbury( 28 ) from the Poway conglomerate of California. Additional species have been figured by G. D. Hanna and M. A. Hanna ( 49 ) from the Eocene of Cowlitz River, Washington. A notable change in foraminiferal assemblage occurs at the base of zone A-3. The faunas of the subjacent five zones are all...

...Robert L. McMaster; John D. Milliman; Asaf Ashraf Abstract Sediments on the continental shelf off Portuguese Guinea, Guinea, and Sierra Leone are mainly terrigenous, and have been stream derived. Except for a lobe of terrigenous material extending seaward from the Orango Delta, most sediments...

... thesis, McMaster University , Hamilton, Canada , 140 p. McCrory , V. L. C. , and R. G. Walker , 1986 , A storm and tidally-influenced prograding shoreline—Upper Cretaceous Milk River Formation of southern Alberta, Canada : Sedimentology , v. 33 , p. 47 – 60 . McLean , D. J...

... and deposition near the few continental rivers, are caused by differential erosion of exposed resistant continental strata on the shallow shelf ( McMaster and Lachance, 1968 ; Emery, 1968 ). South of the deep Cayar Canyon head at 15° N, the shelf is highly reflective ( Fig. 4 , profile A), incised more...

... Cairn. Amphipora ramosa and related species appear to be potentially useful for paleocurrent studies within Devonian carbonate complexes. 1 Manuscript received April 15, 1974. 2 Department of Geology, McMaster University, Hamilton 16, Ontario. This contribution is part of a Master...

... ILURIAN SHALES FROM SOUTH WESTERN ONTARIO GRAHAIV I J. CANDY 1963, McMaster University, M.Sc. A stratigraphie analysis of the Queenston (Ordovician) and Med ina (Silurian) Format ions of southern Ontario, based upon detailed measurement of seventeen sections, shows that these fo rmat ions constitute...

... as paleosols, and crossbedded fluvial channel sandstones. The nonmarine sediments thicken from a zero edge in the northeast to over 40 m in the southwest. Three areas of gravelly shoreface were identified in the study area, and three more are known beyond it. Each is thought to indicate proximity to a river...